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Black Mammoth Metals Finds Large Chargeability Anomaly Underlying Historic Kimmel Mine at Leadore Silver-Lead-REE Property, ID
Black Mammoth Metals Finds Large Chargeability Anomaly Underlying Historic Kimmel Mine at Leadore...
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[{"type":"text","content":"\n\n\n\n Black Mammoth Metals Finds Large Chargeability Anomaly Underlying Historic Kimmel Mine at Leadore Silver-Lead-REE Property, ID\n \n\n /* Style Definitions */\nspan.prnews_span\n{\nfont-size:8pt;\nfont-family:\"Arial\";\ncolor:black;\n}\na.prnews_a\n{\ncolor:blue;\n}\nli.prnews_li\n{\nfont-size:8pt;\nfont-family:\"Arial\";\ncolor:black;\n}\np.prnews_p\n{\nfont-size:0.62em;\nfont-family:\"Arial\";\ncolor:black;\nmargin:0in;\n}\n \n\n\n\n\n\n Canada NewsWire\n \n\n\n\n\n\n\n\n\n\n\n\n BMM: TSX-V\n \n\n\n\n\n VANCOUVER, BC\n \n\n ,\n \n\n June 24, 2025\n \n\n /CNW/ -\n \n Black Mammoth Metals Corporation\n \n (TSXV: BMM) (OTC: LQRCF)\n \n (\"Black Mammoth\" or the \"Company\")\n \n is pleased to announce the results of a recently conducted induced polarization survey (the \"Survey\") at its Leadore Silver-Lead-REE property (\"Leadore\") in\n \n Lemhi County, Idaho\n \n . The Survey's objective was to investigate the area within the historic\n \n Leadore\n \n camp (the \"Leadore Camp\") for a sulfide association, specifically underneath the historic mines: Kimmel,\n \n Leadville\n \n and\n \n Baby Joe\n \n . Intrusive related systems and other deposit types often exhibit an association with sulfides, which produce characteristic chargeability and resistivity responses.\n \n\n\n\n Survey Results:\n \n\n\n\n The IP survey has delineated a large chargeability anomaly with coincident low-resistivity (the \"Anomaly\") within the carbonate host rocks underlying the historic Kimmel mine (see Figure 1)\n \n .\n \n\n The Kimmel also shares a known silver-lead mineralized NW trending fault with the Anomaly where three major fault intersections are adjacent to the Anomaly on the south side. At the center of the Leadore Camp, the Kimmel was reportedly the most productive historic mine. The historical mining data and recent drilling results indicate that sulfide-bearing ores remain open along the NW trending fault and at adjacent fault intersections, which are situated at the base of the Beaverhead mountains and below pediment cover. The maximum east-west width of the Anomaly is estimated at\n \n 400m\n \n and the depth from surface to the top of the Anomaly is estimated at 200 -\n \n 250m\n \n with an overlying silver-lead oxide layer and potentially a placer rare earth element (\"REE\") mineralized layer. The historic Kimmel mine ...